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Koji Iwano, Naohisa Takagaki, Ryoichi Kurose and Satoru Komori. 2013. Mass transfer velocity across the breaking air–water interface at extremely high wind speeds. Tellus B 2013, 65, 21341, http://dx.doi.org/10.3402/tellusb.v65i0.21341

Three velocities of u*, U 10 and U were mistakenly overestimated by 9~19% in the evasion experiments. The mass transfer velocity k L and correct velocities listed in Table 1 should be used in all figures excluding figures 1 and 7. The correct correlations of eqs. (9), (10) and (11) between velocities and mass transfer velocity should be replaced by:

9
kL={76.94u* (u *<1.70)21.62u*3,4(u*1.70)'
10
kL={1.61U101.25(U10<33.6)8.43×10-4U103.4(U1033.6)'
11
kL={1.54U1.5(U<19.3)4.17×10-2U2.72(U19.3).

Fig. 10

Comparison of k L against U between laboratory and field measurements. Symbols and lines as in Fig. 8. A solid line shows the correct correlation curve of eq. (11) normalized to Sc=660 for the present laboratory measurements.

Table 1. Mass transfer velocity and correct velocities

u* (m/s)U10 (m/s)U (m/s)kL (cm/h)0.1494.793.8111.00.2998.386.0721.80.48712.48.4031.90.70416.610.747.80.96721.413.369.81.5931.918.51382.0139.823.92342.4147.729.94253.0259.739.6923

Eventually, the correlation between k L and U almost corresponds to the correlation curve of Wanninkhof and McGillis (1999) at high wind speeds as shown in the correct figure 10.

Language: English
Page range: 25233 - 25233
Published on: Jan 1, 2014
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services

© 2014 none none, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.